TY - JOUR
T1 - Aerosol optical properties at Pasadena, CA during CalNex 2010
AU - Thompson, Jonathan E.
AU - Hayes, Patrick L.
AU - Jimenez, Jose L.
AU - Adachi, Kouji
AU - Zhang, Xiaolu
AU - Liu, Jiumeng
AU - Weber, Rodney J.
AU - Buseck, Peter R.
N1 - Funding Information:
The authors thank Joost de Gouw, Jochen Stutz, Jason Surratt, John Seinfeld, and J.L. Jimenez, the organizers of the CalNex-LA effort, for their service to the community. We also thank Martin Graus and Joost de Gouw for providing the meteorological data presented. Caltech hosted the measurement site. P. Massoli and A. Freedman have provided aerosol extinction coefficients made via a cavity attenuated phase shift (CAPS) instrument for comparison. The entire CalNex community of scholars fostered a collaborative and stimulating environment during the campaign. The California Air Resources Board (CARB) and the National Oceanic & Atmospheric Administration (NOAA) provided funds to help establish the research site. We acknowledge the use of TEM facilities within the LeRoy Eyring Center for Solid State Science at Arizona State University. Special thanks to Kevin Durkee of South Coast Air Quality Management District for providing gravimetric PM data. The TEM study was supported by NSF grants ATM0531926 and ATM1032312 . K. A. acknowledges support from the global environment research fund of the Japanese Ministry of the Environment ( A-1101 ). J.E.T.'s work has been funded in part by the State of Texas/Texas Tech University and in part by NSF grants ATM-0634872 and ATM-1004114 . J.L.J. and P.L.H. acknowledge support from CARB 08-319 and DOE (BER/ASR Program) DE-SC0006035 . P.L.H. acknowledges a CIRES visiting postdoctoral fellowship. R.J.W.'s work was funded through an NSF grant under contract number ATM-0931492 .
PY - 2012/8
Y1 - 2012/8
N2 - Aerosol optical properties measured at the Pasadena, CA site during the CalNex field campaign in May-June 2010 are summarized. Average measurements of PM 2.5 aerosol extinction, scattering, absorption coefficients, and single scattering albedo (b ext, b scat, b abs and SSA) at λ = 532 nm were 62 Mm -1, 58 Mm -1, 4 Mm -1, and 0.92, respectively. The aerosol optical densities were 5 times lower than during the SCAQS study in 1987, highlighting major progress in PM control in the Los Angeles area in the last two decades. The period May 30-June 8 2010 was characterized by exceptionally high aerosol loading (b ext up to 250 Mm -1). During this period, b ext, b scat, and SSA tended to peak during the mid-morning. Correlation of PM 2.5 b ext, b scat with mass concentration data yielded mass scattering and mass extinction coefficients of 3.5-5.1 m 2 g -1 for 532 nm. Aerosol b abs were compared directly to mass concentration of elemental carbon (EC) yielding a campaign average mass absorption cross section (M.A.C.) of 5.7 ± 1.8 m 2 g -1. TEM analysis of particles suggests soot was often internally mixed or adhering to sulfate and/or organics. Total non-refractory PM 1 mass was a good quantitative indicator of coated soot fraction. Alteration of M.A.C. with mixing/coating state was not detected, however, increases in M.A.C. were linked to the presence of light absorbing, water-soluble organic carbon (WSOC) suggesting a possible role of this material invisible light absorption in the LA basin.
AB - Aerosol optical properties measured at the Pasadena, CA site during the CalNex field campaign in May-June 2010 are summarized. Average measurements of PM 2.5 aerosol extinction, scattering, absorption coefficients, and single scattering albedo (b ext, b scat, b abs and SSA) at λ = 532 nm were 62 Mm -1, 58 Mm -1, 4 Mm -1, and 0.92, respectively. The aerosol optical densities were 5 times lower than during the SCAQS study in 1987, highlighting major progress in PM control in the Los Angeles area in the last two decades. The period May 30-June 8 2010 was characterized by exceptionally high aerosol loading (b ext up to 250 Mm -1). During this period, b ext, b scat, and SSA tended to peak during the mid-morning. Correlation of PM 2.5 b ext, b scat with mass concentration data yielded mass scattering and mass extinction coefficients of 3.5-5.1 m 2 g -1 for 532 nm. Aerosol b abs were compared directly to mass concentration of elemental carbon (EC) yielding a campaign average mass absorption cross section (M.A.C.) of 5.7 ± 1.8 m 2 g -1. TEM analysis of particles suggests soot was often internally mixed or adhering to sulfate and/or organics. Total non-refractory PM 1 mass was a good quantitative indicator of coated soot fraction. Alteration of M.A.C. with mixing/coating state was not detected, however, increases in M.A.C. were linked to the presence of light absorbing, water-soluble organic carbon (WSOC) suggesting a possible role of this material invisible light absorption in the LA basin.
KW - Absorption coefficient
KW - Absorption enhancement
KW - Aerosol optics
KW - Albedometer
KW - Brown carbon
KW - CalNex
KW - Direct climate forcing
KW - Extinction coefficient
KW - Mass absorption cross section
KW - Mass scatter efficiency
KW - Scattering coefficient
KW - Single scatter albedo
KW - WSOC
UR - http://www.scopus.com/inward/record.url?scp=84859883672&partnerID=8YFLogxK
U2 - 10.1016/j.atmosenv.2012.03.011
DO - 10.1016/j.atmosenv.2012.03.011
M3 - Article
AN - SCOPUS:84859883672
SN - 1352-2310
VL - 55
SP - 190
EP - 200
JO - Atmospheric Environment
JF - Atmospheric Environment
ER -